Study of acoustic emission signals during fracture shear deformation

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We study acoustic manifestations of different regimes of shear deformation of a fracture filled with a thin layer of granular material. It is established that the observed acoustic portrait is determined by the structure of the fracture at the mesolevel. Joint analysis of the activity of acoustic pulses and their spectral characteristics makes it possible to construct the pattern of internal evolutionary processes occurring in the thin layer of the interblock contact and consider the fracture deformation process as the evolution of a self-organizing system.

作者简介

A. Ostapchuk

Institute of Geosphere Dynamics

编辑信件的主要联系方式.
Email: ostapchuk@idg.chph.ras.ru
俄罗斯联邦, Leninskii pr. 38/1, Moscow, 119334

D. Pavlov

Institute of Geosphere Dynamics

Email: ostapchuk@idg.chph.ras.ru
俄罗斯联邦, Leninskii pr. 38/1, Moscow, 119334

V. Markov

Institute of Geosphere Dynamics

Email: ostapchuk@idg.chph.ras.ru
俄罗斯联邦, Leninskii pr. 38/1, Moscow, 119334

A. Krasheninnikov

Institute of Geosphere Dynamics

Email: ostapchuk@idg.chph.ras.ru
俄罗斯联邦, Leninskii pr. 38/1, Moscow, 119334

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